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Multi-height observations of magnetoacoustic cut-off frequency in a sunspot atmosphere

机译:太阳黑子大气中磁声截止频率的多高度观测

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Context. The cut-off frequency of magnetoacoustic gravity (MAG) waves could be decreased by the inclined magnetic field, and therefore, low-frequency waves could penetrate into the upper atmosphere. Aims. We observe the distribution of the cut-off frequency of compressive waves at various heights and reconstruct the magnetic field inclination, according to the MAG wave theory in a stratified atmosphere permeated by a uniform magnetic field. Methods. We analysed the emission intensity oscillations of sunspot AR11131 (08 Dec. 2010) observed at the 1700 ?, 1600 ?, and 304 ? bandpasses of the Atmospheric Imaging Assembly (AIA) onboard the Solar Dynamics Observatory (SDO), and computed the narrow-band power maps with the pixelised wavelet filtering method. The distribution of the cut-off frequency was defined as the median contour in the azimuthally-averaged oscillation power. The magnetic field inclination was estimated with the local cut-off frequency according to the MAG wave theory in the low-β limit and was compared to the potential field extrapolation. Results. Shorter period oscillations dominate in the sunspot umbra, while longer period oscillations form an annular shape approximately concentric with the sunspot. Oscillations with longer periods are distributed further away from the sunspot centre. The 5 min oscillations appear to originate at or lower than the photosphere. The magnetic field inclinations determined with the cut-off frequency theory are about 30?40% larger than the values obtained by the potential field extrapolation. Conclusions. The oscillation power distribution in a sunspot atmosphere reflects its magnetic and thermal structure. The cut-off frequency could be used to probe the magnetic field inclination, however, other factors have to be included to fully understand this phenomenon. The existence of return magnetic flux at the outer penumbra was evidenced by the cut-off frequency distribution.
机译:上下文。倾斜磁场会降低磁声重力波的截止频率,因此低频波会渗透到高层大气中。目的根据MAG波理论,我们观察了在不同高度下压缩波的截止频率的分布,并重构了磁场倾斜度,这种磁场倾斜是在均匀磁场渗透的分层大气中进行的。方法。我们分析了在1700°,1600°和304°处观测到的黑子AR11131(2010年12月8日)的发射强度振荡。太阳动力学天文台(SDO)上大气成像组件(AIA)的带通,并使用像素化小波滤波方法计算了窄带功率图。截止频率的分布定义为方位角平均振荡功率的中值轮廓。根据低β极限中的MAG波理论,使用局部截止频率估算磁场倾角,并将其与势场外推法进行比较。结果。较短周期的振荡在黑子本影中占主导地位,而较长周期的振荡形成与黑子大致同心的环形形状。周期较长的振荡分布在离黑子中心更远的地方。 5分钟的振荡似乎起源于或低于光球。用截止频率理论确定的磁场倾角比通过势场外推法获得的值大大约30%至40%。结论。太阳黑子大气中的振荡功率分布反映了其磁和热结构。截止频率可以用来探测磁场的倾斜度,但是,必须包括其他因素才能充分理解这种现象。截止频率分布证明了在外半影处存在返回磁通量。

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